magma series mantle Flashcards

1
Q

reflects the isotopic signature of the primitive mabtle as it would evolve to the present w/o any subsequent fractionation of the radioactive elements extracted to form continental and oceanic crust

A

BSE Bulk Silicate Earth

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2
Q

high pb 206/ Pb 204 ration suggestive of a source with high au but it is not enriched in Rb low Sr87/Sr86 old enough >1 Ga to develop the observed isotopic ratios by radioactive decay over time

A

HIMU (High myu)

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3
Q

high He3 and He 4 mantle reservoir act as a mixing conponent and explain the spread of OIB data in the He Sr Nd Pb systems

A

PHEM primitive Helium Mantle

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4
Q

represents a restricted isotopic range tht is common in ocean volcanic rocks

A

PREMA (Prevalent Mantle)

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5
Q

a high He3/He4 component lying approx midway between DM and HIMU that representd actual source material (a true mantle reservoir) or the partial melting process in rising OIB diapirs wc sampla a mixed DM-HIMU source in very consistent proportions

A

FOZO Focal Zone

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6
Q

restricted intermediate isotopic value where the convergence of Pb Nd Sr isotopic data for MORB and OIBs approaches a high He3/ He4 reservoirs

A

Common Mantle

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7
Q

source of N type MORB

A

DM reservoir

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8
Q

less wnriched and may also represent a crustal componentn either ancient oceanic crust or pelagic sediment or they may possibly have been entiched by intra mantle processes stranded melts or metasomatizing fluids

A

EMI and HIMU reservoirs

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9
Q

contain non depleted BSE partially depleted PREMA and non degassed FOZO PURM and C

A

OIB

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10
Q

region along the immediate plate boundary eithin wc volcanism is concentrated is also assoc with very high heat flow indicating an elevated geothermal gradient

A

neovolcanic zone

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11
Q

locus of considerable earthquake activity

A

ridge axis

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12
Q

formed where hydrothermal fluids in excess of 350 C cool dramatically upob escaping from vents and precipitate a number of minerlas including barite silica and several valuable metal sulfides

A

spires chimneys

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13
Q

subduction rate of island arc

A

0.9-10.8 cm/yr

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14
Q

arc type crust range

A

from 12-36 km
averages about 36km

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15
Q

stable only if the melt contains >3 wt. % H2O excess of 0.1 to 0.2 Gpa

A

black hornblende

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16
Q

correspond to steey dipping 25-30 seents of yhe subducting slab

A

active volcanic zones

17
Q

correspond to zegments with much dhallowet dips 10-15 degrees of a segmented Nazca plate

A

inactive volcanic zones

18
Q

originates from the fluid fluxed and LIL enriched mantle wedge above the subducting and dehydrating Nazca plate jn the same manner

A

andean magmatism

19
Q

extends for about 1000km and corresponds to the length of the juan de fuca plate system subducting obliquely beneath the north american plate

A

cascade magmatic arc

20
Q

100-300km long by 10-25 km wife tectonic slices of mafic to silicic volcaniclastic clastic and chemical sediments some tectonic melanges

A

greenstone belts

21
Q

alkali picrite

A

ankaramite

22
Q

co2 rich and less potassic than group 2 kimberlite

A

group I kimberlite

23
Q

h2o rich and has a mica rich matrix

A

group II kimberlite (orangeite)

24
Q

also known alkali basalts lamprophyres alpine peridotites 1-1.4 g percton and occur only underlain by rocks older than 2.5 Ga

A

diamonds

25
Q

dikes near the top into lenticular enlargement up to 10-20 times the file width and 100 m long

A

blows

26
Q

revised term for epiclastic

A

resedimented volcaniclastic kimberlite RVK

27
Q

revised term for tuff ring

A

pyroclastic kimberlite PK

28
Q

revised term for tuffisitic kimberlite breccia TKB

A

massive volcaniclastic kimberlite MVK

29
Q

generated by low degrees of partial melting of hydrated carbonated peridotite

A

kimberlites

30
Q

what were the original shallow water supracrustal sediments

A

politic schists quartzites and marbles

31
Q

mantle xenoliths from kimberlites record pressures up to 4 GPa >120 km but are given igneous names

A

lherzolite

32
Q

critical point of pure h2o is at 374 C and 21.8 MPa

A

hmm

33
Q

resulting metamorhic rocks thus tyicalky display nearly random textural favrics and may generally be called

A

granofels

hornfels if hard and compact

34
Q

muscovite is absent and plag and ortho are common

A

granulite

35
Q

mica rich mylonite

A

phyllonite

36
Q

impact craters may have macroscopic nested cone like structures

A

shatter cones